
Early in the “space race” of the 1950’s, US Air Force Research Laboratory meteorologist and “rocket design climatologist” Norman Sissenwine “recognized the urgent need for complete data on the properties of the atmosphere” and thus became “a catalyst between the aerospace and meteorological community” to develop the US Standard Atmosphere physical model of Earth’s atmospheric pressure, density, and temperature profile by altitude from the surface all the way up to the edge of space at ~100,000+ meters altitude.











